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USE OF AIRBORNE HYPERSPECTRAL DATA IN THE SIMULATION OF SATELLITE IMAGES

机译:在卫星图像仿真中使用空中高光谱数据

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development phase of most Earth Observation missions. This simulation uses frequently as starting point images acquired from airborne instruments. These instruments provide the required flexibility in acquisition parameters (time, date, illumination and observation geometry…) and high spectral and spatial resolution, well above the target values (as required by simulation tools). However, there are a number of important problems hampering the use of airborne imagery. One of these problems is that observation zenith angles (OZA), are far from those that the misisons to be simulated would use. We examine this problem by evaluating the difference in ground reflectance estimated from airborne images for different observation/illumination geometries. Next, we analyze a solution for simulation purposes, in which a Bidirectional Reflectance Distribution Function (BRDF) model is attached to an image of the isotropic surface reflectance. The results obtained confirm the need for reflectance anisotropy correction when using airborne images for creating a reflectance map for simulation purposes. But this correction should not be used without providing the corresponding estimation of BRDF, in the form of model parameters, to the simulation teams.
机译:大多数地球观测特派团的发展阶段。该模拟通常用作从机载仪器获取的起点图像。这些仪器提供了采集参数(时间,日期,照明和观察几何形状......)和高光谱和空间分辨率的所需灵活性,远高于目标值(根据仿真工具的要求)。但是,妨碍了空气传播图像的使用存在许多重要问题。其中一个问题是观察天顶角(OZA),远非那些被模拟的误解会使用的角度。我们通过评估来自空中图像估计的地面反射率的差异来检查该问题,用于不同观察/照明几何形状。接下来,我们分析用于仿真目的的解决方案,其中双向反射率分布函数(BRDF)模型附着在各向同性表面反射率的图像上。当使用空气载体图像以产生用于模拟目的时,确认了在使用空中图像时,确认需要反射各向异性校正。但是,不应使用这种校正,而无需以模型参数的形式提供BRDF的相应估计,到模拟团队。

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